{"id":92270,"date":"2026-06-29T14:35:46","date_gmt":"2026-06-29T12:35:46","guid":{"rendered":""},"modified":"2026-07-08T15:08:19","modified_gmt":"2026-07-08T13:08:19","slug":"0198cc808f21-3dd3307d-6c19-465e-872c-eec30d41ea47","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/0198cc808f21-3dd3307d-6c19-465e-872c-eec30d41ea47\/","title":{"rendered":"Transport of mercury in the Arctic atmosphere: Evidence for a springtime net sink and summer-time source"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-08 14:34:15","footnotes":""},"nva_tax_category":[1059],"class_list":["post-92270","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-scientific-journal-publication"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/92270","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication"}],"about":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/types\/nva_publication"}],"version-history":[{"count":1,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/92270\/revisions"}],"predecessor-version":[{"id":92271,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/92270\/revisions\/92271"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=92270"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=92270"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}